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  2. Fractofusus misrai - Wikipedia

    en.wikipedia.org/wiki/Fractofusus_misrai

    Fractofusus misrai is an Ediacaran fossil discovered in 1967 by S.B. Misra at Mistaken Point, Newfoundland and Labrador, Canada, which has since become the Mistaken Point Ecological Reserve. [1] It was named after Professor Misra in 2007. [2]

  3. Mistaken Point Ecological Reserve - Wikipedia

    en.wikipedia.org/wiki/Mistaken_Point_Ecological...

    The first fossil to be found in the area, Fractofusus misrai, was discovered in June 1967 by Shiva Balak Misra, an Indian graduate student studying geology at Memorial University of Newfoundland. [ 3 ] [ 4 ] In the mid-1980s, the site quickly became recognized as an important location containing possibly the oldest metazoan fossils in North ...

  4. Princeton Chert - Wikipedia

    en.wikipedia.org/wiki/Princeton_Chert

    The Princeton Chert is a fossil locality in British Columbia, Canada, which comprises an anatomically preserved flora of Eocene Epoch age, with rich species abundance and diversity. It is located in exposures of the Allenby Formation on the east bank of the Similkameen River , 8.5 km (5.3 mi) south of the town of Princeton, British Columbia .

  5. Category:Fossils of Canada - Wikipedia

    en.wikipedia.org/wiki/Category:Fossils_of_Canada

    Fossil museums in Canada (2 C, 6 P) Pages in category "Fossils of Canada" The following 200 pages are in this category, out of approximately 215 total.

  6. Mistaken Point Formation - Wikipedia

    en.wikipedia.org/wiki/Mistaken_Point_Formation

    In the summer of 1967, Shiva Balak Misra, an Indian graduate student (1966–69) at Newfoundland's Memorial University discovered a rich assemblage of imprints of soft bodied organisms on the surface of large rock slabs, while mapping the Conception Group of Avalon Peninsula of Newfoundland near Cape Race, at a place called Mistaken Point.

  7. Burgess Shale - Wikipedia

    en.wikipedia.org/wiki/Burgess_Shale

    The Burgess Shale is a fossil-bearing deposit exposed in the Canadian Rockies of British Columbia, Canada. [ 2 ] [ 3 ] It is famous for the exceptional preservation of the soft parts of its fossils. At 508 million years old ( middle Cambrian ), [ 4 ] it is one of the earliest fossil beds containing soft-part imprints.

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